锦屏一级水电站左岸抗力体基础处理洞室群围岩稳定性分析
投稿时间:2009-06-08  修订日期:2009-08-17  点此下载全文
引用本文:王胜,黄润秋,祝华平.锦屏一级水电站左岸抗力体基础处理洞室群围岩稳定性分析[J].钻探工程,2009,36(9):72-76.
WANG Sheng,HUANG Run-qiu,ZHU Hua-ping. Analysis on Stability of Surrounding Rock of Underground Chamber Group on Left Bank Resisting Rock of Jinping-I Hydropower[J]. Drilling Engineering, 2009,36(9):72-76.
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作者单位E-mail
王胜* 成都理工大学地质灾害防治与地质环境保护国家重点实验室 yongyuandewangsheng@sina.com 
黄润秋 成都理工大学地质灾害防治与地质环境保护国家重点实验室  
祝华平 中国水电顾问集团成都勘测设计研究院  
中文摘要:通过对锦屏一级水电站左岸抗力体五层洞室岩体结构特征详细调查,采用水电围岩分类的方法对抗力体洞室进行围岩分类。分类结果表明:抗力体洞室围岩以Ⅲ2类围岩居多,占了50%左右,其次为Ⅳ类,占36%左右,Ⅲ1和Ⅴ类围岩所占比例较少。通过对洞室施工开挖失稳破坏现象的调查研究,分析了洞室失稳破坏的机制及破坏形式,认为围岩主要的破坏形式为弱面控制型的块体滑移塌落。对洞室监测资料的分析结果表明,在目前的支护条件下,总体监测未见异常,整体上基础处理洞室监测状态稳定。但F5、F42-9断层及煌斑岩脉等软弱部位应力及变形缓慢增加,需要加强监测。最后根据分析结果提出了建议。
中文关键词:抗力体  围岩分类  破坏机制  块体  监测  稳定性
 
Analysis on Stability of Surrounding Rock of Underground Chamber Group on Left Bank Resisting Rock of Jinping-I Hydropower
Abstract:By the detailed survey on the structure features of left bank resisting rock of Jinping-I hydropower, resisting rock chambers were classified with surrounding rock classification. 50% resisting rock chambers belong to Ⅲ2, about 36% belong to Ⅳ, and the rest belong to Ⅲ1 and Ⅴ. By the study on excavating destabilization, analysis was made on the stability-loosing mechanism and the deformation pattern. Weak-plane-controlling block gliding and collapsing were thought to be the main deformation pattern. According to the analysis on the chamber monitoring data, no evidence showed any abnormal; but deformation of F5, F42-9 faults and lamprophyre dyke were slowly occurred. The paper put forward the construction proposal.
keywords:resisting rock  surrounding rock classification  destruction mechanism  block  monitoring  stability
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